CO2Carbon dioxide storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment estimations of European hydrocarbon fields have been carried out in the GESTCO (Schuppers et al., 20032003 - J. D. Schuppers, S. Holloway, F. May, P. Gerling, G. Boe, C. Magnus, F. Riis, P. T. Osmundsen, M. Larsen, P. R. Andersen and G. HatziyannisStorage capacity and quality of hydrocarbon structures in the North Sea and Aegean region'see more) and the EUEuropean Union GeoCapacity projects (Vangkilde-Pedersen et al., 2008). For all fields, the equivalent of practical or realistic capacity was assessed. These were static capacities estimated on the assumption that the volume occupied by recoverable hydrocarbons (recovery ratio as using standard production technology, without CO2Carbon dioxide injectionThe process of using pressure to force fluids down wells) in the reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids can be filled up again by injected carbon dioxide. For a number of case studies, injectionThe process of using pressure to force fluids down wells scenarios were analysed, and the equivalent of matched or practical capacity was obtained.
Especially in the case of gas fields, the formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it factor - i.e. the volume produced gas occupies in the reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids divided by its volume on at the surface - is essential to provide a reliable estimate of static CO2Carbon dioxide storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment (see Fig. 2-7, density of natural gasGas stored underground; It consists largely of methane, but can also contain other hydrocarbons, water, hydrogen sulphide and carbon dioxide, these other substances are separated before the methane is put into a pipeline or tanker within the reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids is 100-300 kg/m3, while at the surface is less than 1 kg/m3).
Fig. 2-7: Density variation of natural gasGas stored underground; It consists largely of methane, but can also contain other hydrocarbons, water, hydrogen sulphide and carbon dioxide, these other substances are separated before the methane is put into a pipeline or tanker and CO2Carbon dioxide with depth (Schuppers et al., 20032003 - J. D. Schuppers, S. Holloway, F. May, P. Gerling, G. Boe, C. Magnus, F. Riis, P. T. Osmundsen, M. Larsen, P. R. Andersen and G. HatziyannisStorage capacity and quality of hydrocarbon structures in the North Sea and Aegean region'see more). |
The following, simplified formula was used in order to estimate the static capacities of hydrocarbon fields (Schuppers et al., 20032003 - J. D. Schuppers, S. Holloway, F. May, P. Gerling, G. Boe, C. Magnus, F. Riis, P. T. Osmundsen, M. Larsen, P. R. Andersen and G. HatziyannisStorage capacity and quality of hydrocarbon structures in the North Sea and Aegean region'see more; Tab. 2-5):
MCO2Carbon dioxide = ρCO2r × URp × B
The capacity can also be calculated using Bachu, 20082008 - S. BachuCO2 storage in geological media: Role, means, status and barriers to deploymentsee more Phase III formula:
MCO2Carbon dioxide = rCO2r × (Rf × OOIP / Bf - Viw + Vpw)
where OOIP is original oil in place.
In this last expression, URp in fact represents Rf OGIP and Rf OOIP, respectively, but the formula does not take Fig, Viw and Vpw into account. URp is the sum of the cumulative production and the proven reserves and typically, the methodology for calculating/estimating the proven reserves varies from country to country.
Tab. 2-5: Parameters used in the static capacity assessment of hydrocarbon fields (GESTCO and EUEuropean Union GeoCapacity projects; Schuppers et al., 20032003 - J. D. Schuppers, S. Holloway, F. May, P. Gerling, G. Boe, C. Magnus, F. Riis, P. T. Osmundsen, M. Larsen, P. R. Andersen and G. HatziyannisStorage capacity and quality of hydrocarbon structures in the North Sea and Aegean region'see more and Vangkilde-Pedersen et al., 2008). Parameter | MCO2Carbon dioxide | ρCO2r | URp | B | Description | Hydrocarbon field storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment | CO2Carbon dioxide density at reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids conditions | Proven ultimate* recoverable oil or gas | Oil or gas formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it factor | Typical values | Oil & Gas: Mtonnes to hundreds of Mtonnes | 0.6-0.8 g/cm3 | Oil - Mm3 (106 m3) to hundreds of Mm3 Gas - Bm3 (109 m3) to hundreds of Bm3 | Oil - slightly bigger than 1; Gas - far smaller than 1 (e.g. 0.003-0.007) | *For gas fields in case gas is re-injected the amount shall be extracted from URp; Regarding URp of oil fields where water is injected and produced the injected one shall decrease and the produced increase URp. |
The ultimate recoverable oil and gas can be given, on a field by field basis, as the sum of produced volumes and expected reserves, or by applying a fixed conversion factor to the expected ultimate recoverable oil and gas.
The formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it volume factor used for oil varies regionally and/or locally depending on the oil type and the formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it volume factor used for gas should vary with depth as a function of pressure and temperature. Likewise the CO2Carbon dioxide density should also vary with depth as a function of pressure and temperature. Both may, however, in some countries, have been applied as constant average values to all hydrocarbon fields.
The methodology used for hydrocarbon fields yields theoretical storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment, according to the methodology described by Bachu et al., 20072007 - S. Bachu, D. Bonijoly, J. Bradshaw, R. Burruss, N. P. Christensen, S. Holloway and O. M. MathiassenEstimation of CO2 Storage Capacity in Geological Media – Phase 2. Work under the auspices of the Carbon Sequestration Leadership Forumsee more. To reach effective storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment, a number of capacity coefficients representing mobility, buoyancyTendency of a fluid or solid to rise through a fluid of higher density, heterogeneity, water saturation and aquiferAn underground layer of fluid-bearing permeable rock or unconsolidated materials (gravel, sand, or silt) with significant permeability to allow flow strength were introduced, all of which reduce the storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment. However, if there are insufficient data for estimating the values of these capacity coefficients, it is not possible to distinguish between theoretical and effective storage(CO2Carbon dioxide) A process for retaining captured CO2Carbon dioxide, so that it does not reach the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) capacityThe accumulated mass of CO2Carbon dioxide that can be stored environmentally safely, i.e., without causing leakage(in CO2Carbon dioxide storage) The escape of injected fluid from the storage formationA body of rock of considerable extent with distinctive characteristics that allow geologists to map, describe, and name it to the atmosphereThe layer of gases surrounding the earth; the gases are mainly nitrogen (78%) and oxygen (around 21%) or water column of CO2Carbon dioxide or native reservoirA subsurface body of rock with sufficient porosityMeasure for the amount of pore spaceSpace between rock or sediment grains that can contain fluids in a rock and permeabilityAbility to flow or transmit fluids through a porous solid such as rock to store and transmit fluids fluids or triggering geologic activity that has a negative impact on human health or the environment for hydrocarbon fields.